首页> 外文期刊>Current Microbiology: An International Journal >Compositions and structures of archaeal communities in Acid mineral bioleaching systems of dongxiang copper mine and yinshan lead-zinc mine, china.
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Compositions and structures of archaeal communities in Acid mineral bioleaching systems of dongxiang copper mine and yinshan lead-zinc mine, china.

机译:东乡铜矿山和银山铅锌矿山酸性矿物生物浸出系统中古细菌群落的组成和结构

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Four samples were studied from four separated sites with heap leaching in the Yinshan Lead-Zinc Mine and the Dongxiang Copper Mine in Jiangxi province, China. The compositions and structures of archaeal communities in four sites were identified by a polymerase chain reaction-based cloning approach. A total of six operational taxonomic units (OTUs) was obtained from four samples. The highest percentage of overlapped OTUs was 88.9% between sites DX and D1. Phylogenetic analysis revealed that archaea in the four acid mineral bioleaching systems fell into two divisions: Thermoplasma and Ferroplasma. The proportions of Thermoplasma and Ferroplasma in all four sites were 20.6% and 79.4%, respectively. The proportions of clones clustered with Ferroplasma in four sites were 93.8% (D1), 30.5% (D3), 100% (DY), and 93.2% (DX), respectively. The proportions of clones clustered with Thermoplasma in the other three sites were 6.2% (D1), 69.5% (D3), and 6.8% (DX), respectively. The results of principal component analysis based on the percentages of six OTUs obtained from four sites and geochemical data from four sites suggested that the concentrations of elements such as lead, cobalt, and sulfur might be the reason causing the different archaeal structure in site D3 than those in the other three sites.
机译:在中国江西省银山铅锌矿和东乡铜矿,从四个分离的地点进行了四个样品的堆浸研究。通过基于聚合酶链反应的克隆方法鉴定了四个部位的古细菌群落的组成和结构。从四个样本中总共获得了六个操作分类单位(OTU)。站点DX和D1之间重叠OTU的最高百分比为88.9%。系统发育分析表明,四种酸性矿物生物浸出系统中的古细菌分为两个部分:热质体和铁质体。在所有四个部位中,热浆和铁质的比例分别为20.6%和79.4%。在四个位点上与铁质体聚集的克隆的比例分别为93.8%(D1),30.5%(D3),100%(DY)和93.2%(DX)。在其他三个位点上与Thermoplasma聚集的克隆的比例分别为6.2%(D1),69.5%(D3)和6.8%(DX)。基于从四个地点获得的六个OTU的百分比和四个地点的地球化学数据的主成分分析结果表明,铅,钴和硫等元素的浓度可能是导致地点D3中的古细菌结构不同的原因。其他三个站点中的站点。

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